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74 Nw eifuku Volcano, Champagne vent. The white-smoker chimneys are ~ 20-cm across and ~ 50-cm high, and venting fluids measure 103°C. white flocculent mats and elemental sulfur coatings surround the chimneys, and liquid Co 2 droplets rise from the seafloor. Measurements of conductive heat flow typically fall below predictions of lithospheric cooling models until an average lithospheric age of ~ 65 Ma. This deviation from model predictions, and the variability of seafloor heat flow commonly observed on ridge flanks, is generally attributed to hydrothermal circulation. This circulation also contributes to geochemical reactions that facilitate the exchange of solutes between the crust and ocean, redistribute elements within the crust, and alter the physical state of plates as they

Seamounts as Conduits for Massive Fluid, Heat, and Solute Fluxes on Ridge Flanks